The possibility that microorganisms might use reduced humic substances (hum
ics) as an electron donor for the reduction of electron accepters with a mo
re positive redox potential was investigated. All of the Fe(III)- and humic
s-reducing microorganisms evaluated were capable of oxidizing reduced humic
s and/or the reduced humics analogue anthrahydroquinone-2,6,-disulphonate (
AHQDS), with nitrate and/or fumarate as the electron acceptor. These includ
ed Geobacter metallireducens, Geobacter sulphurreducens, Geothrix fermentan
s, Shewanella alga, Wolinella succinogenes and 'S. barnesii', Several of th
e humics-oxidizing microorganisms grew in medium with AHQDS as the sole ele
ctron donor and fumarate as the electron acceptor. Even though it does not
reduce Fe(III) or humics, Paracoccus denitrificans could use AHQDS and redu
ced humics as electron donors for denitrification, However, another denitri
fier, Pseudomonas denitrificans, could not. AHQDS could also serve as an el
ectron donor for selenate and arsenate reduction by W. succinogenes, Electr
on spin resonance studies demonstrated that humics oxidation was associated
with the oxidation of hydroquinone moieties in the humics, Studies with G.
metallireducens and W. succinogenes demonstrated that the anthraquinone-2,
6-disulphonate (AQDS)/AHQDS redox couple mediated an interspecies electron
transfer between the two organisms. These results suggest that, as microbia
lly reduced humics enter less reduced zones of soils and sediments, the red
uced humics may serve as electron donors for microbial reduction of several
environmentally significant electron accepters.